Electromagnetic Geothermometry /

Electromagnetic Geothermometry explores, presents and explains the new technique of temperature estimation within the Earth's interior; the Electromagnetic technique will identify zones of geothermal anomalies and thus provides locations for deep drilling. This book includes many case studies f...

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Bibliographic Details
Main Authors: Spichak, V. V. (Vi︠a︡cheslav Valentinovich) (Author), Zakharova, Olga K. (Author)
Corporate Author: ScienceDirect (Online service)
Format: eBook
Language:English
Published: Amsterdam, Netherlands : Elsevier, [2015]
Subjects:
Online Access:Connect to the full text of this electronic book

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245 1 0 |a Electromagnetic Geothermometry /  |c Viacheslav V. Spichak, Olga K. Zakharova. 
264 1 |a Amsterdam, Netherlands :  |b Elsevier,  |c [2015] 
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504 |a Includes bibliographical references and index. 
520 |a Electromagnetic Geothermometry explores, presents and explains the new technique of temperature estimation within the Earth's interior; the Electromagnetic technique will identify zones of geothermal anomalies and thus provides locations for deep drilling. This book includes many case studies from geothermal areas such as Travale (Italy), Soultz-sous-Forêts (France) and Hengill (Iceland), allowing the author and reader to draw conclusions regarding the dominating heat transfer mechanisms, location of its sources and to constrain the locations for drilling of the new boreholes. Covering a topic that so far has very little coverage (due to its newness) Electromagnetic Geothermometry presents ground breaking information on the interpretation of MT signals. And as such, is similar to the work that was done to develop new generations of seismic inversion methods that have since come to dominate the oil industry. Up until now geophysical methods have had difficulty resolving temperature differences which have been critical in the understanding of location and magnitude of geothermal resources Authored by the world's foremost geothermometry experts who combined have more than 40 years of experience on the subject Presents case studies, allowing the author and reader to draw conclusions regarding the dominating heat transfer mechanisms, location of its sources and to constrain the locations for drilling of the new boreholes Provides important information on the constraints for drilling of new exploration boreholes Describes techniques that will dramatically decrease the costs associated with exploration drilling Includes information to help the reader improve the accuracy of the temperature estimations in the interwell space as well as far beneath boreholes. 
505 0 |a Cover; Title Page; Copyright Page; Contents; Preface; Part I -- Methodology; Chapter 1 -- Electromagnetic Sounding of Geothermal Areas; 1.1 -- Introduction; 1.2 -- Conceptual models of geothermal areas; 1.3 -- Factors affecting electrical resistivity of rocks; 1.3.1 -- Temperature; 1.3.2 -- Rock Porosity and Permeability; 1.3.3 -- Alteration Mineralogy; 1.4 -- Imaging of geothermal areas; 1.4.1 -- MT Sounding; 1.4.2 -- Other EM Methods; 1.4.3 -- 3-D Resistivity Models of Geothermal Zones; 1.5 -- EM footprints of thermotectonics, faulting, and fracturing; 1.6 -- Monitoring of the target macroparameters 
505 8 |a 1.7 -- Using of geological and other geophysical data1.8 -- Constraining locations for drilling boreholes; 1.9 -- Conclusions; References; Chapter 2 -- Techniques Used for Estimating the Temperature of the Earth's Interior; 2.1 -- Temperature models based on the boreholes' logs and the heat flow data; 2.2 -- Temperature estimations using indirect geothermometers; 2.2.1 -- Mineral Geothermometers; 2.2.2 -- Hydrochemical Geothermometers; 2.2.3 -- Gas Geothermometers; 2.2.4 -- Isotopic Geothermometers; 2.2.5 -- Geothermometers Based on the Seismicity Bounds 
505 8 |a 2.3 -- Interplay between the electromagnetic sounding data, rock physics, and prior geological information2.4 -- Technique for the deep temperature model building using the global magnetovariational sounding data and guess about t...; 2.4.1 -- Analysis of the Mantle Temperature Models; 2.4.2 -- An Updated Formula for Deep Electrical Conductivity; 2.4.3 -- The Temperature Model of the Mantle; 2.5 -- Conclusions; References; Chapter 3 -- Neural Network Approach to the Temperature Estimation; 3.1 -- Introduction; 3.2 -- ANN with a teacher (backpropagation technique); 3.3 -- Testing of the ANN 
505 8 |a 3.3.1 -- Analytical Temperature Model of the Geothermal Reservoir3.3.2 -- Effect of the Data Volume; 3.3.3 -- Effect of the "Geographic" Factor; 3.4 -- An example of the neural network based temperature forecast in the geothermal area; 3.4.1 -- Data; 3.4.2 -- Effect of the Temperature Logs' Number; 3.4.3 -- Effect of the Temperature Logs' Type; 3.5 -- Conclusions; References; Chapter 4 -- Indirect Electromagnetic Geothermometer; 4.1 -- General scheme of the electromagnetic geothermometer; 4.2 -- EM Temperature Interpolation in the interwell space; 4.2.1 -- Effect of the Data Volume 
505 8 |a 4.2.2 -- Effect of the Neuronet Training Strategy4.2.3 -- Effect of the Geology and Hydrological Conditions; 4.3 -- EM temperature extrapolation in depth; 4.3.1 -- Sedimentary Cover; 4.3.1.1 -- Data and Thermometer Calibration; 4.3.1.2 -- Temperature Extrapolation; 4.3.2 -- Geothermal Area; 4.3.2.1 -- Data and Thermometer Calibration; 4.3.2.2 -- Temperature Extrapolation; 4.3.3 -- Robustness Evaluation; 4.4 -- Conclusions; References; Part II -- Case Studies; Chapter 5 -- Estimation of the Deep Temperature Distribution in the Chu Depression (Northern Tien Shan) 
505 8 |a 5.1 -- Geological setting and the regime of the underground waters 
650 0 |a Temperature measurements. 
650 0 |a Electromagnetic waves. 
650 6 |a Thermométrie. 
650 6 |a Ondes électromagnétiques. 
650 7 |a electromagnetic radiation.  |2 aat 
650 7 |a SCIENCE  |x Mechanics  |x Thermodynamics.  |2 bisacsh 
650 7 |a Electromagnetic waves  |2 fast 
650 7 |a Temperature measurements  |2 fast 
650 7 |a Temperaturmessung  |2 gnd 
650 7 |a Erdinneres  |2 gnd 
650 7 |a Elektromagnetische Messung  |2 gnd 
650 7 |a Geothermik  |2 gnd 
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